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Home
Science
Environmental Science
Earthquakes II: Strain and Faults
Faults
faults: a large brittle fracture in a rock body
the point of origin for most earthquakes
Terminology
movement range along a break in a rock body is fractions of an inch to miles
fractures: fractions of inches to inch movements
faults: feet to mile movements
plate boundaries: contacts between tectonic plates
Normal Fault
blocks move away from each other
hanging wall block moves down relative to foot wall
Reverse (or Thrust) Fault
blocks move towards each other
hanging wall block moves up relative to foot wall
Strike-Slip Fault
motion is lateral (like traffic driving)
fault itself is vertical (no hanging wall or foot wall blocks)
Types of Strike-Slip Faults
left-lateral: movement relatively to the left
right-lateral: movement relatively to right
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